Boreal soil homogenization after conversion to agricultural use is constrained by carbon dynamics and soil health

• Farming converted boreal soil led to swift homogenization to agricultural benchmarks. • Accelerated soil respiration was linked to high soil C and low compaction. • Farmed low fertility boreal Podzols may behave like slash and burn agriculture. • Management focused on soil C could regenerate these soils for long-term C storage. As climate changes progress, land use conversion (LUC) intensifies in boreal regions, fuelling concerns that post-LUC farming may cause further decline in soil carbon (C) by altering C pools and degrading soil health. However, detailed data on how boreal soils respond after LUC to agriculture remains scarce. This study addresses this gap by analysing a representative farm in Happy Valley-Goose Bay in Labrador, Canada converted from mixed boreal spruce forest and sphagnum peat bog between 2013 and 2018. C concentrations were measured in a grid pattern across a 0–5 year management chronosequence at two depths (0–15 and 15–30 cm). Time-partitioned burst respiration (24 h intervals) was used to assess the soil’s functional status in relation to changes in background and management-altered physicochemical factors. Respiration patterns closely followed total soil C and nitrogen, and were significantly affected by compaction, indicating that C levels, moderated by hydrology, drive respiration in converted sandy Podzols. Soils shifted toward what might be argued are agricultural norms within five years: higher respiration and pH, and increased uniformity of C/N, phosphorus, aluminium, iron, magnesium, and manganese concentrations. Variability in soil function was most strongly linked to soil C, as high-C soil resisted homogenization but supported vigorous crop growth, while homogenized low-C soil struggled to support plants. This study demonstrates that C loss post-conversion in boreal Podzols is a clear danger to soil fertility in spite of rapid homogenization to agricultural norms.

Authors

Institutions

Publication Details

Journal
CATENA
Published
2025-10-22
DOI
https://doi.org/10.1016/j.catena.2025.109553
Primary Topic
Soil Carbon and Nitrogen Dynamics
Type
article
Field-Weighted Citation Impact
0.00
Controls
|||
ALL TIME
JAN
FEB
MAR
APR
MAY
JUN
JUL
AUG
SEP
OCT
article

Boreal soil homogenization after conversion to agricultural use is constrained by carbon dynamics and soil health

Daniel Altdorff, Jeremiah D. Vallotton, Lakshman Galagedara, Adrian Unc
CATENA
Soil Carbon and Nitrogen Dynamics
article

Boreal soil homogenization after conversion to agricultural use is constrained by carbon dynamics and soil health

Daniel Altdorff, Jeremiah D. Vallotton, Lakshman Galagedara, Adrian Unc
article en

Abstract

• Farming converted boreal soil led to swift homogenization to agricultural benchmarks. • Accelerated soil respiration was linked to high soil C and low compaction. • Farmed low fertility boreal Podzols may behave like slash and burn agriculture. • Management focused on soil C could regenerate these soils for long-term C storage. As climate changes progress, land use conversion (LUC) intensifies in boreal regions, fuelling concerns that post-LUC farming may cause further decline in soil carbon (C) by altering C pools and degrading soil health. However, detailed data on how boreal soils respond after LUC to agriculture remains scarce. This study addresses this gap by analysing a representative farm in Happy Valley-Goose Bay in Labrador, Canada converted from mixed boreal spruce forest and sphagnum peat bog between 2013 and 2018. C concentrations were measured in a grid pattern across a 0–5 year management chronosequence at two depths (0–15 and 15–30 cm). Time-partitioned burst respiration (24 h intervals) was used to assess the soil’s functional status in relation to changes in background and management-altered physicochemical factors. Respiration patterns closely followed total soil C and nitrogen, and were significantly affected by compaction, indicating that C levels, moderated by hydrology, drive respiration in converted sandy Podzols. Soils shifted toward what might be argued are agricultural norms within five years: higher respiration and pH, and increased uniformity of C/N, phosphorus, aluminium, iron, magnesium, and manganese concentrations. Variability in soil function was most strongly linked to soil C, as high-C soil resisted homogenization but supported vigorous crop growth, while homogenized low-C soil struggled to support plants. This study demonstrates that C loss post-conversion in boreal Podzols is a clear danger to soil fertility in spite of rapid homogenization to agricultural norms.

CATENAVol. 261
Memorial University of Newfoundland (CA), University of Potsdam (DE), McGill University (CA)
Openalex Percentile: Top 62%
Soil Carbon and Nitrogen Dynamics
AI Navigator

Ask Laika to Summarize, Analyze, and Connect papers live on the map.

Summarize Papers & Methodologies

Extract key findings, datasets, and comparative methods across publications.

Benchmark Rankings & Visual Analytics

Rank top research institutions, authors, funders, topics, and journals by Field-Weighted Citation Impact (FWCI) and paper volume with instant charts.

Connect Distant Disciplines

Bridge topological clusters on the map to find hidden collaborative intersections.